Srinivasan, M. S. (1965) Eocene-Oligocene boundary in New Zealand Nature, 207 . pp. 514-515. ISSN 0028-0836
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Official URL: http://www.nature.com/nature/journal/v207/n4996/ab...
Related URL: http://dx.doi.org/10.1038/207514a0
Abstract
The planktonic foraminifera Hantkenina, Globigerapsis and Pseudohastigerina micra are widely distributed throughout the world and their last appearance has generally been considered to mark the top of the Eocene. Hornibrook stated that H. alabamensis, G. index and P. micra make their last appearance in the Runangan Stage, and consequently regarded the Runangan-Whaingaroan boundary as the Eocene-Oligocene boundary in New Zealand.
| Item Type: | Article |
|---|---|
| Source: | Copyright of this article belongs to Nature Publishing Group. |
| ID Code: | 51168 |
| Deposited On: | 28 Jul 2011 07:28 |
| Last Modified: | 28 Jul 2011 07:28 |
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